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SEISMIC ANALYSIS OF WATER SUPPLY SYSTEMS BY EARTHQUAKE<br />

SCENARIO SIMULATION<br />

Gee-Yu LIU, Chin-Hsun YEH, Hsiang-Yuan HUNG and Kuang-Wu CHOU<br />

National Center for Research on <strong>Earthquake</strong> Engineering, Taiwan<br />

ABSTRACT: In the past decade, scenario simulation has played a more and more important role in urban<br />

earthquake hazard mitigation and emergency response. Both public and private sectors can be enhanced in<br />

terms <strong>of</strong> their seismic preparedness and operation if adequate implementation <strong>of</strong> seismic scenario simulation<br />

can be employed. Regarding water utilities, system-wide retr<strong>of</strong>it and emergency planning can be conducted<br />

to reduce the likely damage and losses prior to the occurrence <strong>of</strong> a devastating earthquake. Post-earthquake<br />

repair personnel and material dispatching, temporary water supply for affected people, emergency water<br />

supply for hospitals and fire fighting, strategies for restoration and recovery can all benefit from<br />

scenario-based analyses. In this research work, efforts were made to study and integrate pivotal technologies<br />

essential to the earthquake damage and serviceability analysis <strong>of</strong> water systems, such as seismic hazard<br />

analysis, empirical formulae for pipe repair rates, hydraulic analysis <strong>of</strong> water network system in terms <strong>of</strong><br />

pressurized pipe flow simulation, hydraulic models for various types <strong>of</strong> pipe damages, and Monte Carlo<br />

method for the performance analysis <strong>of</strong> large and complicated systems. The water system in Yi-lan County,<br />

Taiwan was selected as a test bed for the demonstration <strong>of</strong> its seismic serviceability analysis under an M7.1<br />

earthquake scenario.<br />

KEYWORDS: water system, post-earthquake performance, scenario simulation<br />

1. INTRODUCTION<br />

<strong>Water</strong> systems are one <strong>of</strong> the most essential<br />

infrastructures in modern societies. The disruption <strong>of</strong><br />

water supply following earthquakes may cause<br />

serious inconvenience to the daily life <strong>of</strong> people in<br />

the disastrous areas. Medical caring, sanitation,<br />

fire-fighting and so forth may be seriously affected,<br />

too. It is very important to facilitate water utilities<br />

with a seismic scenario simulation tool for help<br />

estimate the likely service disruption following<br />

earthquakes. Such tool will benefit the efforts to<br />

improve preparedness, robustness, and resilience <strong>of</strong><br />

water systems in a quantitative approach. In the past<br />

years, Shinozuka et al. (1981), Ballantyne et al.<br />

(1990) and Markov et al. (1994) have made pioneer<br />

studies in this topic. Recently, s<strong>of</strong>tware called<br />

GIRAFFE (Graphical Iterative Response <strong>Analysis</strong><br />

for Flow Following <strong>Earthquake</strong>s) has been<br />

developed at Cornell University (2008). It was<br />

successfully adopted as a decision support tool for<br />

hazard mitigation and emergency response <strong>by</strong> the<br />

Los Angele Department <strong>of</strong> <strong>Water</strong> and Power. It<br />

employs EPANET as the engine for hydraulic<br />

computation. EPANET is public computer codes<br />

released <strong>by</strong> the Environmental Protection Agency,<br />

U.S., especially for the solution <strong>of</strong> pressurized pipe<br />

flow problem (Rossman, 2000).<br />

Similar to GIRAFFE, a technology for assessing


the post-earthquake performance <strong>of</strong> water systems<br />

has been developed at NCREE (Liu et al., 2010 &<br />

2011). It consists <strong>of</strong> several steps, as depicted in<br />

Figure 1. (1) estimate the seismic hazards (ground<br />

shaking and failure) <strong>of</strong> where the interested water<br />

network system locates, (2) simulate the locations <strong>of</strong><br />

pipe damages according to the hazards and pipe<br />

repair rates (numbers <strong>of</strong> repairs per unit pipe length<br />

caused <strong>by</strong> ground shaking and deformation,<br />

respectively), (3) classify the properties <strong>of</strong> each pipe<br />

damage (whether a break or a leak, and what which<br />

model <strong>of</strong> pipe leak if it is a leak; the probability<br />

model for pipe damages employed <strong>by</strong> GIRAFFE was<br />

adopted here), (4) modify the hydraulic model <strong>of</strong> the<br />

water network system to take into account the pipe<br />

damages, (5) execute EPANET and take out the<br />

water supply nodes affected <strong>by</strong> negative pressure<br />

from the solution. Details <strong>of</strong> these steps will be<br />

explained in the following sections.<br />

EQ source parameters<br />

ground motion attenuation<br />

site effect<br />

fault rupturing model<br />

liquefaction susceptibility<br />

liquefaction settlement model<br />

pipe repair rate<br />

pipe damage locating algorithm<br />

equipment vulnerability<br />

power outage<br />

…<br />

pipe damage hydraulic models<br />

EPANET s<strong>of</strong>tware<br />

pre- and post-processors<br />

EQ Event<br />

<strong>Seismic</strong> Hazards<br />

Ground<br />

Ground<br />

Shaking<br />

Failure<br />

Numbers <strong>of</strong><br />

Damage<br />

Pipe Damage<br />

and<br />

Malfunction<br />

Locations <strong>of</strong><br />

<strong>of</strong><br />

Pipe Damage<br />

Equipment<br />

Hydraulic <strong>Analysis</strong><br />

System Serviceability<br />

Figure 1 Flowchart for the serviceability assessment<br />

<strong>of</strong> water systems following earthquakes<br />

2. PIPE DAMAGE MODELING<br />

Repair rate (RR) is defined as the number <strong>of</strong> repairs<br />

(or damages) per unit pipe length (km). It is widely<br />

employed to indicate pipe fragility under seismic<br />

effects. Numerous investigations have been made to<br />

express the relationship between pipe repair rate and<br />

earthquake-induced ground shaking (e.g. peak<br />

ground acceleration, PGA) or ground failure (e.g.<br />

permanent ground displacement, PGD). The pipe<br />

material and diameter affect its repair rate, too. The<br />

empirical formulae for pipe repair rates have been<br />

proposed <strong>by</strong> the authors, which read (Liu et al.,<br />

2011):<br />

RR = C ⋅ RR 0<br />

RR<br />

0<br />

where<br />

RR PGA<br />

RR PGD<br />

= max[ RR ,RR ] + RR<br />

PGA<br />

=<br />

= 0.6445 ⋅ PGD<br />

PGDFault<br />

−3<br />

6.5756 × 10 ⋅ ( PGA −<br />

0.728<br />

PGDLiq<br />

100)<br />

0.878<br />

⋅ p<br />

where RR<br />

0<br />

is the standard pipe repair rate, C is<br />

an adjustment coefficient and is a function <strong>of</strong> pipe<br />

material and diameter, PGA and PGD are in<br />

cm/sec 2 and cm, respectively. The terms<br />

PGDFault<br />

,<br />

PGD<br />

Liq<br />

and p<br />

Liq<br />

represent the fault<br />

rupturing and soil liquefaction-induced PGDs, and<br />

the probability <strong>of</strong> occurrence <strong>of</strong> soil liquefaction,<br />

respectively.<br />

Conventionally, a stationary Poisson process is<br />

widely used to simulate the damage locations along a<br />

pipe. In this study, an approach based on the<br />

expected number <strong>of</strong> damages <strong>of</strong> pipes was otherwise<br />

proposed. From Figure 2, let the length <strong>of</strong> a typical<br />

pipe segment be L . Assume there are a total <strong>of</strong> N<br />

pipes in the water pipe network under study. Let all<br />

pipes be broken down into segments <strong>of</strong> constant<br />

length L from their beginning nodes (the length <strong>of</strong><br />

the last segment <strong>of</strong> each pipe may not equal L ), and<br />

be denoted as ( i , j)<br />

, where i refers to pipe i<br />

( i = 1,..., N ) and j refers to its j -th segment. The<br />

expected number <strong>of</strong> pipe damage <strong>of</strong> any pipe<br />

segment ( i , j)<br />

can be decided according to the<br />

segment length and the corresponding pipe repair<br />

Liq


ate. Denote this number as e ij<br />

. Starting with the<br />

origin <strong>of</strong> the number line, if all the expected numbers<br />

<strong>of</strong> pipe damage e<br />

11<br />

, e12,...,<br />

e21,<br />

e22,...,<br />

e NJ<br />

(where<br />

N<br />

J<br />

N<br />

refers to the last segment <strong>of</strong> pipe N ) can be<br />

sequentially accumulated as ( e 11<br />

), ( e<br />

11<br />

+ e12<br />

),<br />

( e ),<br />

11<br />

+ e12<br />

+ e13 ...,(<br />

e<br />

11<br />

+ e12<br />

+ ... + e NJ<br />

) and denoted<br />

N<br />

on the number line, then the interval [ 0, E<br />

R<br />

] , where<br />

E<br />

R<br />

equals to the summation <strong>of</strong> all the expected<br />

numbers <strong>of</strong> pipe damage, consists <strong>of</strong> as many<br />

sub-intervals as the number <strong>of</strong> all pipe segments with<br />

lengths e<br />

11<br />

, e12,...,<br />

e21,<br />

e22,...,<br />

e NJ<br />

. This also means<br />

N<br />

that there exists a one-on-one mapping between any<br />

real-number within [ 0, E<br />

R<br />

] and a specific pipe<br />

segment.<br />

were adopted in this study. This model includes pipe<br />

break and various types <strong>of</strong> pipe leaks, and the<br />

probability that each will occur in various pipe<br />

materials, and also the hydraulic models and<br />

parameters for each type <strong>of</strong> pipe damage. Following<br />

their findings from water pipelines and their<br />

damages in past earthquakes in the U.S., water pipe<br />

materials could be classified into 5 types: cast iron,<br />

ductile iron, jointed concrete, riveted steel and<br />

welded steel. Furthermore, there are five different<br />

types <strong>of</strong> pipe leaks, namely the annular<br />

disengagement, round crack, longitudinal crack,<br />

local loss <strong>of</strong> pipe wall, and local tear <strong>of</strong> pipe wall at<br />

welded slip joint, as illustrated in Figure 3.<br />

Conventional approach:<br />

Assume that pipe damage follows a Poisson process<br />

Proposed approach:<br />

0<br />

Accumulated<br />

number <strong>of</strong> pipe<br />

damage points<br />

E R<br />

Generate a random number within [0, E R ], designate the location, and repeat E R times<br />

Figure 2 Comparison between the conventional and<br />

the proposed approaches for simulating pipe damage<br />

locations probabilistically<br />

To simulate a location <strong>of</strong> damage along the pipe,<br />

first, an arbitrary number between 0 and E<br />

R<br />

can be<br />

generated using a random number generator that<br />

follows uniform distribution. It will refer to one<br />

single segment, say e nm<br />

, along the axis <strong>of</strong> number<br />

line. Finally, the midpoint <strong>of</strong> the m -th segment <strong>of</strong><br />

the n -th pipe is designated as a pipe damage<br />

location. The same process can be repeated E R<br />

times to determine all pipe damage locations.<br />

The hydraulic models for pipe damages<br />

proposed in GIRAFFE (Cornell University, 2008)<br />

Figure 3 Schematic diagrams <strong>of</strong> the 5 types <strong>of</strong> pipe<br />

leaks (Cornell University, 2008)<br />

GIRAFFE further proposed the hydraulic models<br />

for pipe breaks and leaks, respectively. A pipe break<br />

and its hydraulic model can be depicted as the left<br />

schematic diagram in Figure 4. At each <strong>of</strong> the broken<br />

ends, a reservoir and a short pipe with a check valve<br />

are needed being added to mimic the mechanism <strong>of</strong><br />

water flowing into the atmosphere. To take into<br />

account the effect <strong>of</strong> a pipe break in simulation,<br />

several steps to modify the hydraulic model <strong>of</strong> the<br />

broken water system should be taken. They are: (1)<br />

Decide the location and elevation <strong>of</strong> pipe break point,<br />

(2) Remove the original link (pipe segment), (3) Add<br />

two new nodes A and B at the location <strong>of</strong> pipe break<br />

point, (4) Add two new links connecting the original


pipe segment ends to A and B, respectively, (5) Add<br />

two new nodes A’ and B’ with the elevation <strong>of</strong> pipe<br />

break point and designate them as reservoirs, and<br />

finally (6) Add two new links connecting A-A’ and<br />

B-B’ and specify them with one-way check valves.<br />

Figure 5 Hydraulic model for a pipe leak (Cornell<br />

University, 2008)<br />

3. HYDRAULIC ANALYSIS AND NEGATIVE<br />

PRESSURE ISSUE<br />

Figure 4 Hydraulic model for a pipe break (Cornell<br />

University, 2008)<br />

On the other hand, a pipe leak and its hydraulic<br />

model could be depicted as the right schematic<br />

diagram in Figure 5. A pipe leak is hydraulically<br />

equivalent to a sprinkler with a specific discharge<br />

coefficient and an orifice size. This sprinkler is<br />

further proven to be equivalent to a fictitious pipe<br />

linking the original pipe and an added reservoir. A<br />

check valve is designated to the fictitious pipe<br />

ensuring that water flows from the leaking pipe to<br />

the reservoir. The steps to modify the hydraulic<br />

model <strong>of</strong> the leaking water system could be<br />

summarized as follows: (1) Decide the location and<br />

elevation <strong>of</strong> pipe leak point, (2) Remove the original<br />

link (pipe segment), (3) Add a new node A at the<br />

location <strong>of</strong> pipe leak point, (4) Add two new links<br />

connecting the original pipe segment ends to A, (5)<br />

Add a new node A’ with the elevation <strong>of</strong> pipe leak<br />

point and designate it as a reservoir, and finally (6)<br />

Add a new link connecting A and A’ and specify it as<br />

a fictitious pipe with a diameter <strong>of</strong> corresponding<br />

pipe leak model, and also specify it with a one-way<br />

check valve.<br />

Figure 6 depicts the schematic diagram <strong>of</strong> a<br />

simplified water network. A water network system<br />

usually consists <strong>of</strong> tanks, reservoirs, pumps, valves<br />

and numerous pipes and nodes. The hydraulics <strong>of</strong><br />

such a system can be assumed as pressurized pipe<br />

flows, and can be solved <strong>by</strong> using two sets <strong>of</strong><br />

equations (Rossman, 2000). Let there be N nodes,<br />

NF fixed nodes (e.g. tanks and reservoirs) and K<br />

pipes in a water network, then the first set prescribe<br />

the difference <strong>of</strong> water head at the ends <strong>of</strong> each pipe<br />

and read:<br />

H − H<br />

i<br />

j<br />

= h<br />

ij<br />

= r ⋅Q<br />

n<br />

ij<br />

+ m ⋅Q<br />

where H , h ,Q , r , n and m are the nodal head, head<br />

loss, flow rate, resistance coefficient, flow exponent<br />

and minor loss coefficient, respectively. The most<br />

widely used empirical formulae for the pipe<br />

resistance coefficient are the Darcy-Weisbach,<br />

Hazen-Williams or Chezy-Manning equation, all <strong>of</strong><br />

which employ flow rate and various pipe parameters.<br />

The second set prescribes the balance <strong>of</strong> flow at each<br />

node and read:<br />

∑<br />

j<br />

Q − D = 0<br />

ij<br />

i<br />

2<br />

ij


where<br />

D<br />

i<br />

is the demand at node i . By using these<br />

two sets <strong>of</strong> equations, the pipe flow can be solved in<br />

terms <strong>of</strong> the water heads H<br />

i<br />

at N nodes and the<br />

pipe flow rate Q (from node j to node i ) in<br />

K pipes.<br />

ij<br />

(4) Perform hydraulic analysis using EPANET.<br />

(5) Check the pressure at all nodes from the result <strong>of</strong><br />

Step (4) and, following the approach proposed <strong>by</strong><br />

Ballantyne et al. (1990) to eliminate the negative<br />

pressure and summarize the water supply <strong>by</strong><br />

excluding the demands (supplies) at nodes <strong>of</strong><br />

negative pressure.<br />

Read input file for the hydraulic<br />

analysis <strong>of</strong> the water system<br />

Figure 6 The schematic diagram <strong>of</strong> a simplified<br />

hydraulic network (Rossman, 2000)<br />

The procedure for assessing the post-earthquake<br />

performance <strong>of</strong> a water system is illustrated in the<br />

flowchart in Figure 7, which reads:<br />

Modify input file according to<br />

the simulated pipeline damage<br />

Pipeline damage causes<br />

any node disconnected<br />

from the system network<br />

YES<br />

Remove the disconnected nodes<br />

NO<br />

(1) Read the input file for the hydraulic analysis <strong>of</strong><br />

the interested water system. This file is usually<br />

prepared <strong>by</strong> the water utilities and is compatible<br />

with the employed analysis s<strong>of</strong>tware in terms <strong>of</strong><br />

data formatting. All attributes <strong>of</strong> the components<br />

in the water system (e.g. reservoirs, tanks, pumps,<br />

nodes and pipes) are defined in the file.<br />

(2) Simulate the pipeline damage <strong>of</strong> the water system<br />

based on an earthquake scenario. A pre-processor<br />

has been developed in this study to decide the<br />

locations and attributes <strong>of</strong> pipe breaks and leaks<br />

in the pipeline network in a probabilistic way, and<br />

then to modify the input file according to the<br />

simulated pipeline damage. It takes into account<br />

the seismic hazard and the pipe repair rate, and<br />

the pipe damage models Proposed in GIRAFFE<br />

(Cornell University, 2008) were employed.<br />

(3) Check the connectivity <strong>of</strong> all nodes to the system<br />

with simulated pipeline damage. Remove the<br />

disconnected nodes <strong>by</strong> further modifying the<br />

input file.<br />

Pre-processor<br />

Perform hydraulic<br />

analysis using EPANET<br />

Post-processor<br />

Negative pressure<br />

NO<br />

occurs at any node<br />

YES<br />

Remove water supply at nodes <strong>of</strong> negative pressure<br />

Evaluate the serviceability <strong>of</strong> the damaged water system<br />

End<br />

Figure 7 Flowchart for assessing post-earthquake<br />

performance <strong>of</strong> a water system<br />

While performing hydraulic analysis <strong>of</strong> a water<br />

network with pipe damage, it is likely to predict<br />

negative pressure at some nodes. Negative pressure<br />

is generated due to the assumption that the pipe<br />

flows are always full and pressurized. However,<br />

water pipelines are not air-tight, especially when


they are damaged. As a result, hydraulic analysis <strong>of</strong> a<br />

damaged water network tends toward overestimating<br />

its ability to convey water. Elimination <strong>of</strong> negative<br />

pressure under such circumstance is therefore<br />

advised. In this study, the approach proposed <strong>by</strong><br />

Ballantyne et al. (1990), which assumes that no<br />

water will flow through negative pressure nodes, was<br />

employed in Step 5 <strong>of</strong> the assessment procedure.<br />

Pipes<br />

Junctions<br />

Tanks or reservoirs<br />

礁 溪 鄉<br />

員 山 鄉<br />

宜 蘭 市<br />

頭 城 鎮<br />

壯 圍 鄉<br />

4. CASE STUDY<br />

三 星 鄉<br />

五 結 鄉<br />

羅 東 鎮<br />

The <strong>of</strong>f-shore <strong>of</strong> eastern coast is one <strong>of</strong> the most<br />

earthquake-prone areas in Taiwan region. In this<br />

study, the water system in Yi-lan County, one <strong>of</strong> the<br />

three counties in East Taiwan, was chosen as the test<br />

bed for the implementation <strong>of</strong> the proposed ESLE<br />

technology. The water system in Yi-lan County is<br />

operated <strong>by</strong> the Eighth Branch <strong>of</strong> the Taiwan <strong>Water</strong><br />

Corporation. Its service area is 814 kilometer square.<br />

The total pipe length is approximately 2,600 km. The<br />

system serves 150,500 customers or 427,000 people,<br />

with an average supply <strong>of</strong> 162,395 CMD (2010). The<br />

major pipes include PVC pipes (63%), ductile iron<br />

pipes (26%), HIWP (high-impact PVC) pipes (6%)<br />

and cast iron pipes (1%). The entire system is<br />

simplified as a hydraulic node-and-link network,<br />

depicted in Figure 8, with a total <strong>of</strong> 358 nodes and<br />

439 links.<br />

Consider an earthquake occurring <strong>of</strong>f-shore<br />

Yi-lan County. The earthquake magnitude is 7.1, the<br />

epicenter locates at the coordinates <strong>of</strong> ( 121.88<br />

E,<br />

24.28<br />

N ) and the focal depth is 20km. Assume that<br />

the source mechanism is a horizontal line source <strong>of</strong><br />

84.2km with north-south orientation. The ground<br />

shaking and ground failure induced <strong>by</strong> this scenario<br />

earthquake can be simulated <strong>by</strong> TELES and be<br />

illustrated as Figure 9.<br />

冬 山 鄉<br />

蘇 澳 鎮<br />

Figure 8 The water system in Yi-lan County<br />

PGA<br />

PGD ( 土 壤 液 化 )<br />

PGA (g)<br />

PGD (cm)<br />

y<br />

0.54 to 0.6<br />

45 to 50<br />

0.48 to 0.54<br />

40 to 45<br />

0.42 to 0.48<br />

35 to 40<br />

0.36 to 0.42<br />

30 to 35<br />

0.3 to 0.36<br />

25 to 30<br />

0.24 to 0.3<br />

20 to 25<br />

0.18 to 0.24<br />

15 to 20<br />

0.12 to 0.18<br />

10 to 15<br />

0.06 to 0.12<br />

5 to 10<br />

0 to 0.06<br />

0 to 5 (<br />

Figure 9 Simulated distribution <strong>of</strong> PGA (left) and<br />

liquefaction-induced PGD (right) in Yi-lan County<br />

under the M7.1 scenario earthquake<br />

The Monte Carlo method was employed to<br />

estimate the average post-earthquake serviceability<br />

<strong>of</strong> the system. One hundred times <strong>of</strong> simulation were<br />

performed, and the pipe breaks and leaks due to<br />

ground shaking and failure were decided according<br />

to a random process in each run. The simulation<br />

results are depicted in Figure 10. Here, the<br />

serviceability index (SI), defined as the ratio <strong>of</strong> flow<br />

at demand nodes after and before an earthquake, is


used to quantify the system’s ability to meet the<br />

demand in each town. Under this scenario, the worst<br />

reduction in SI occurs in Tou-cheng (0.3521), while<br />

the other two worst reductions occur in Zhuangwei<br />

(0.5091) and Jiao-xi (0.5430), respectively.<br />

Serviceability Index<br />

0 to 0.1<br />

0.1 to 0.2<br />

0.2 to 0.3<br />

0.3 to 0.4<br />

0.4 to 0.5<br />

0.5 to 0.6<br />

0.6 to 0.7<br />

0.7 to 0.8<br />

0.8 to 0.9<br />

0.9 to 1<br />

1 to 1<br />

礁 溪 鄉<br />

頭 城 鎮<br />

system in terms <strong>of</strong> the serviceability index (SI) <strong>of</strong><br />

each service area was simulated.<br />

ACKNOWLEDGEMENT<br />

The research funding from <strong>Water</strong> Resource Agency,<br />

MOEA, Taiwan under Grants MOEA-WRA-<br />

0990095 and MOEA-WRA-1000090 is gratefully<br />

acknowledged. This research was made possible<br />

through kind helps from the Taiwan <strong>Water</strong><br />

Corporation for providing technical assistance and<br />

database.<br />

員 山 鄉<br />

宜 蘭 市<br />

壯 圍 鄉<br />

REFERENCES<br />

三 星 鄉<br />

五 結 鄉<br />

羅 東 鎮<br />

Ballantyne, D. B., Berg, E., Kennedy, J., Reneau, R.<br />

and Wu, D. (1990). <strong>Earthquake</strong> Loss Estimation<br />

大 同 鄉<br />

冬 山 鄉<br />

蘇 澳 鎮<br />

Modeling <strong>of</strong> the Seattle <strong>Water</strong> System, Technical<br />

Report, Kennedy/Jenks/Chilton, Federal Way, WA.<br />

南 澳 鄉<br />

Cornell University. (2008). GIRAFFE User’s<br />

Manual, School <strong>of</strong> Civil & Environmental Eng.,<br />

Cornell University, Ithaca, NY.<br />

Figure 10 The simulated serviceability <strong>of</strong> Yi-lan’s<br />

water system under the M7.1 scenario earthquake<br />

5. CONCLUDING REMARKS<br />

A technology for assessing the seismic performance<br />

<strong>of</strong> water systems has been developed. Key issues<br />

including models <strong>of</strong> strong motion attenuation and<br />

pipe repair rate, and the pipe damage model have<br />

explained. Particularly, a new approach for the<br />

simulation <strong>of</strong> pipe damage locations based on the<br />

expected number <strong>of</strong> damages <strong>of</strong> pipe segment has<br />

been proposed. The water network system in Yi-lan<br />

County, Taiwan was employed as a test bed for case<br />

study. A major earthquake occurring <strong>of</strong>f-shore was<br />

considered. The post-earthquake performance <strong>of</strong> the<br />

Liu, G.-Y., Chung, L.-L., Yeh, C.-H., Wang, R.-Z.,<br />

Chou, K.-W., Hung, H.-Y., Chen, S.-A., Chen, Z.-H.<br />

and Yu, S.-H. (2010). A Study on Pipeline <strong>Seismic</strong><br />

Performance and System Post-<strong>Earthquake</strong> Response<br />

<strong>of</strong> <strong>Water</strong> Utilities (1/2), Technical Report MOEA-<br />

WRA-0990095, <strong>Water</strong> Resource Agency, MOEA,<br />

Taipei.<br />

Liu, G.-Y., Chung, L.-L., Huang, C.-W., Yeh, C.-H.,<br />

Chou, K.-W., Hung, H.-Y., Chen, Z.-H., Chou, C.-H.<br />

and Tsai, L.-C. (2011). A Study on Pipeline <strong>Seismic</strong><br />

Performance and System Post-<strong>Earthquake</strong> Response<br />

<strong>of</strong> <strong>Water</strong> Utilities (2/2), Technical Report MOEA-<br />

WRA-1000090, <strong>Water</strong> Resource Agency, MOEA,<br />

Taipei.


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(1994). An Evaluation <strong>of</strong> <strong>Seismic</strong> Serviceability<br />

<strong>Water</strong> <strong>Supply</strong> Networks with Application to the San<br />

Francisco Auxiliary <strong>Water</strong> <strong>Supply</strong> System, Technical<br />

Report NCEER-94-0001, National Center for<br />

<strong>Earthquake</strong> Engineering Research, Buffalo, NY.<br />

Rossman, L.A. (2000). EPANET 2 User’s Manual,<br />

EPA (U.S. Environmental Protection Agency),<br />

Cincinnati, OH.<br />

Shinozuka, M, Tan, R. Y. and Toike, T. (1981).<br />

Serviceability <strong>of</strong> <strong>Water</strong> Transmission <strong>Systems</strong> under<br />

<strong>Seismic</strong> Risk, Lifeline <strong>Earthquake</strong> Engineering, the<br />

Current State <strong>of</strong> Knowledge, ASCE, New York, NY.<br />

Yeh, C. H., Loh, C.-H. and Tsai, K.C. (2003).<br />

“Development <strong>of</strong> <strong>Earthquake</strong> Assessment Methodology<br />

in NCREE,” Proc. Joint NCREE/JRC Workshop<br />

Int. Collaboration on <strong>Earthquake</strong> Disaster<br />

Mitigation Research, Technical Report NCREE-03<br />

-029, pp.83–92, Taipei.

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